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基于热重分析的菱镁矿分解动力学解析
Decomposition kinetics of magnesite deduced from thermogravimetric analysis

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张强   何宏平   陶奇 *  
文摘 本文利用热重(TG)分析方法,探讨了菱镁矿的热分解过程。根据热微商(DTG)曲线峰顶温度,结合Kissinger及Ozawa-Doyle方法拟合计算得到菱镁矿热分解的活化能和指前因子(lgA)分别为211.55 kJ/mol和11.07 s~(-1)。依次采用单曲线拟合、多元非线性拟合及Malek方法判定得出菱镁矿热分解过程属于三维相界反应模型(R3),其动力学方程为: dα/dT=(10~(11.07)/β)·e~(-211.55×10~3/(8.314×T))·3(1-α)~(2/3)。
其他语种文摘 Decomposition kinetics of magnesite was investigated by using thermogravimetric (TG) analysis. The activation energy (E) and pre-exponential factor (lgA) were calculated from Kissinger and Ozawa-Doyle equations, and the peak value of derivative thermogravimetry (DTG) data was used as the maximum temperature. The calculated E and lgA were 211.55 kJ/mol and 11.07 s~(-1), respectively. The reaction mechanism was further discussed by using single-TG curve, multivariate no-linear regressions and Malek method, respectively. The obtained results indicate that the reaction was a three-dimensional phase boundary reaction (R3). The kinetic equation was as follows: dα/dT=(10~(11.07)/β)·e~(-211.55×10~3/(8.314×T))·3(1-α)~(2/3).
来源 岩石矿物学杂志 ,2014,33(2):391-396 【核心库】
关键词 菱镁矿 ; 热重分析 ; 分解动力学 ; 机理函数1
地址

中国科学院广州地球化学研究所, 广东, 广州, 510640

语种 中文
文献类型 研究性论文
ISSN 1000-6524
学科 地质学
基金 国家自然科学基金 ;  广东省自然科学基金 ;  佛山市院市合作项目
文献收藏号 CSCD:5104097

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